Want this question answered?
Midocean ridges are areas where continents broke apart. Midocean ridges are closest to the landmasses in younger oceans. One example where a midocean ridge intersected a landmass is the Arabian sea, which was formed by the pulling apart of the Arabian Peninsula and Africa.
One of the midocean ridges is, but others are in other oceans, seas, and bays.
The boundary between the asthenosphere and the lithosphere is normally below the Moho (which marks the boundary between the crust and the mantle). The exception to this is below mid-ocean ridges where the moho and the lithosphere / asthenosphere boundary are at the same depth.
The Mid-Atlantic Ridge is found on the ocean floor in the middle of the Atlantic Ocean.
yes
Midocean ridges are areas where continents broke apart. Midocean ridges are closest to the landmasses in younger oceans. One example where a midocean ridge intersected a landmass is the Arabian sea, which was formed by the pulling apart of the Arabian Peninsula and Africa.
Mid-ocean ridges transfer energy from the mantle/asthenosphere/lithosphere to the surface. The energy is from the deep Earth.
At transform faults or transform zones.
One of the midocean ridges is, but others are in other oceans, seas, and bays.
Abyssal plains cover about 50% of the surface area on Earth and usually positioned between continents and midocean ridges. They are typically at least 3000m deep and represent some of the flatest, smoothest, and least explored landscapes on Earth.
Older, as it moves away from the mid-ocean ridge the sediment gets thicker and older
(1)midocean spreading ridges, (2) subduction zones, and (3) transform faults.Normal fault, Reverse fault, and strike-slip fault
Dermal ridges are the surface ridges of the skin of the palms and soles, where the sweat pores open.
We can't yet be certain, but the current best guess is that it is predominantly covered with ice. In fact, one of the interesting theories concerning Europa is that the ridges that we can see on the surface were caused by the ice cracking, and the liquid (water?) beneath boiling into space and then refreezing, and then forming pressure ridges when the ice sheets come back together.
The boundary between the asthenosphere and the lithosphere is normally below the Moho (which marks the boundary between the crust and the mantle). The exception to this is below mid-ocean ridges where the moho and the lithosphere / asthenosphere boundary are at the same depth.
The midocean ridges are the spreading centers where the plates are moving apart. The seamounts are extinct volcanos produced as the plate passed over a mantle hotspot.
The Mid-Atlantic Ridge is found on the ocean floor in the middle of the Atlantic Ocean.